Gordia is an ichnofossil known from Precambrian[1] to modern sediments and is the most common trace fossil in the Kaili biota displaying "smooth, cylindrical or subcylindrical, non-branching, winding and irregularly curving burrows, commonly self-overcrossing".[2] Probably made by a worm-like creature displaying fodinichnial (sediment scavenging) behaviour.[2] It takes the form of unlined, curving parallel-walled burrows that often end with a nub, probably created as the creature probed the over- or under-lying sediment.[2] It resembles Helminthopsis and Haplotichnus.[2]
| Gordia Temporal range:
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Trace fossil classification 
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| Genus: | †Gordia Emmons, 1844 |
References
edit- ^ "Gordia". paleobiodb.org. Retrieved 2023-04-25.
- ^ a b c d Wang, Y.; Lin, J. P.; Zhao, Y. L.; Orr, P. J. (2009). "Palaeoecology of the trace fossil Gordia and its interaction with nonmineralizing taxa from the early Middle Cambrian Kaili Biota, Guizhou Province, South China". Palaeogeography, Palaeoclimatology, Palaeoecology. 277 (1–2): 141–148. Bibcode:2009PPP...277..141W. doi:10.1016/j.palaeo.2009.02.017.
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